Porosity of crushed rock layer and its impact on thermal regime of Qinghai−Tibet Railway embankment-Reference-Cited by-同舟云学术

Porosity of crushed rock layer and its impact on thermal regime of Qinghai−Tibet Railway embankment

Published:2017-04 Issue:4 Volume:24 Page:977-987
ISSN:2095-2899
Container-title:Journal of Central South University
language:en
Short-container-title:J. Cent. South Univ.

Author:

Liu Ming-hao,Li Guo-yu,Niu Fu-jun,Lin Zhan-ju,Shang Yun-hu

Publisher

Springer Science and Business Media LLC

Subject

Metals and Alloys,General Engineering

Link

http://link.springer.com/content/pdf/10.1007/s11771-017-3500-2.pdf

Reference46 articles.

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2. WU Qing-bai, CHENG Guo-dong, MA Wei. Impact of permafrost change on the Qinghai-Tibet Railroad engineering [J]. Science in China: Series D, 2004, 47(suppl 1): 122–130.

3. WU Qing-bai, CHENG Hong-bin, JIANG Guan-li, MA Wei, LIU Yong-zhi. Cooling mechanism of embankment with block stone interlayer in Qinghai-Tibet railway [J]. Science in China: Series E, 2007, 50(3): 319–328.

4. MA Wei, MU Yan-hu, WU Qing-bai, SUN Zhi-zhong, LIU Yong-zhi. Characteristics and mechanisms of embankment deformation along the Qinghai-Tibet Railway in permafrost regions [J]. Cold Regions Science and Technology, 2011, 67(3): 178–186.

5. LAI Yuan-ming, ZHANG Shu-juan, ZHANG Lu-xin, XIAO Jian-zhang. Adjusting temperature distribution under the south and north slopes of embankment in permafrost regions by the ripped rock revetment [J]. Cold Regions Science and Technology, 2004, 39 (1): 67–79.

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